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Professor Shotton asked for amplification of the relationships of the Older Till, which the author dated as Saale , to the later drifts.
A widespread erosional unconformity is recognized throughout the Variscan foreland in mid-Permian time, known as the Saalian unconformity, and this unconformity is prominent in the Grensen Nose area.
Glacial deposits found in the southern part are probably of Saale age, or even older.
The blocking of major river valleys in the Leinebergland area by the Early Saalian Scandinavian ice sheet led to the formation of a large glacial lake.
However, it should be noted that this anticline is partly related to post-Asturic tectonics: the Asturic unconformity is itself truncated by the Saalian unconformity on the crest of the structure.
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